Currents and convection cause enhanced gas exchange in the ice–water boundary layer

Brice LooseGraduate School of Oceanography, University of Rhode Island, 215 South Ferry Rd., Narragansett, RI02882, USACorrespondence[email protected]

Ann LovelyGraduate School of Oceanography, University of Rhode Island, 215 South Ferry Rd., Narragansett, RI02882, USA

Peter SchlosserDepartment of Earth and Environmental Sciences, Columbia University, Room 106 Geosciences Bldg., Palisades, NY10964, USA;Department of Earth and Environmental Engineering, Columbia University, 918 Seeley Mudd Bldg., 500 West 120th St, New York, NY10027, USA;Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, NY10964, USA

Christopher ZappaDepartment of Earth and Environmental Sciences, Columbia University, Room 106 Geosciences Bldg., Palisades, NY10964, USA

Wade McGillisLamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, NY10964, USA

Donald PerovichUS Army Corps of Engineers Cold Regions Research and Engineering Laboratory, 72 Lyme Rd., Hanover, NH03755, USA

Currents and convection cause enhanced gas exchange in the ice–water boundary layer

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Currents and convection cause enhanced gas exchange in the ice–water boundary layer

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